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Record W2799662919

Entrapment and re-equilibration of gold-bearing fluid inclusions (Sigma deposit - Abitibi belt - Canada). A multidisciplinary study.

2005· article· en· W2799662919 on OpenAlexaboutno aff
Paolo Garofalo, Christoph A. Heinrich, D. Guenther, Thomas Pettke

Bibliographic record

VenueArchivio istituzionale della ricerca (Alma Mater Studiorum Università di Bologna) · 2005
Typearticle
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsnot available
Fundersnot available
KeywordsGreenstone beltGeologyEntrapmentFluid inclusionsBearing (navigation)GeochemistrySigmaMining engineeringArcheanSeismologyHydrothermal circulationLawGeographyPolitical science
DOInot available

Abstract

fetched live from OpenAlex

Sigma is a large network of steeply dipping, Au-mineralized quartz-tourmaline-carbonate shear veins and subhorizontal extension veins. We have used 1) petrographic identification of eight fluid inclusions assemblages (FIAs) trapped during quartz, tourmaline, and gold precipitation within the veins; 2) microthermometry; 3) Raman spectroscopy; and 4) Laser Ablation-ICP-MS of single fluid inclusions to determine PTX estimates of the vein fluid. Either an H2O-NaCl-B±CH4-N2 (aqueous) fluid or an H2O-NaCl-CO2-B (aquo-carbonic) fluid is trapped within single FIAs, which are formed by liquid- and vapor-rich inclusions. Within all FIAs, inclusions show specific morphologies. Relatively large inclusions are dendritic, hook-like, and annular, while smaller inclusions are relatively more regular and show sharp tips. In both aqueous and aquo-carbonic fluid types, liquid-rich and vapor-rich inclusions have salinities of 4-8 wt% NaCleq and 0.5-4 wt% NaCleq, respectively. Homogenization occurs into the liquid and vapor phases. In the aquo-carbonic fluid, the carbonic phase melts between -56.5 and -57 °C. Clathrate melts between about 6.0 C and 8.0 °C, and ThCO2 ranges from -12 to 31 °C. The distribution of Thtot within individual FIAs show modes between 330 and 385 °C, but low-temperature outliers are common (ranges: 100-180 °C). These data, inclusion morphologies, and tests for equilibrium coexistence of liquid- and vapor-rich inclusions show that post-entrapment modifications affected the FIAs. We interpret these features as indication of an “implosion” re-equilibration regime, and propose a general method to interpret microthermometric data of heterogeneously trapped fluids in terms of distinct regimes. Following this method, the properties of the high-Thtot inclusions of Sigma are those approaching the pristine fluid. Notably, the selection of these inclusions contrasts with that commonly used for the estimation of the PT trapping conditions of heterogeneously trapped fluids at equilibrium. However, the properties estimated with the high-Thtot inclusions predict gold and tourmaline solubilities that agree with the bulk concentrations of B and Au measured with Laser Ablation-ICP-MS in single fluid inclusions. They also predict a quartz solubility that agrees with that estimated independently. Thus, our data are consistent with gold precipitation within the quartz-tourmaline veins after unmixing of a parent H2O-NaCl-CO2 fluid at about 350-400 °C and 300-500 bars.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.319
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0010.000
Scholarly communication0.0000.000
Open science0.0010.003
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.011
GPT teacher head0.211
Teacher spread0.200 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations1
Published2005
Admission routes1
Has abstractyes

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